Posted on by Tammy Plotner

Russia Opens Talks With NASA And ESA With Plans For Manned Lunar Base

Multiple images of the International Space Station flying over the Houston area have been combined into one composite image to show the progress of the station as it crossed the face of the moon in the early evening of Jan. 4. (Lauren Harnett)

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On January 19, 2012, Roscosmos, the Russian Space Agency began talking to the United States and Europe about the stuff dreams are made of… a manned research base on the Moon. The agency’s chief, Vladimir Popovkin, led off the discussion with officials from NASA and the European Space Agency for a permanent facility. “We don’t want man to just step on the Moon,” Popovkin told Vesti FM radio station, according to the Ria Novosti news agency. “Today, we know enough about it, we know that there is water in its polar areas … we are now discussing how to begin [the Moon’s] exploration with NASA and the European Space Agency.”

But that’s not all. One giant leap for mankind often begins with one small step – or two. In this instance, Russia is planning to launch two unmanned missions to the Moon within the next 8 years. According to Popovkin, the plan is to either set up a stationary base on the lunar surface, or to put a working laboratory into orbit around it.

Don’t shoot these comments down just because they’ve come to light after a recent run of bad luck on behalf of Russia’s current space missions – most notably the doomed Mars probe Phobos-Grunt which crashed back to Earth following a malfunction. According to Fix News, “It was the latest mishap for Roscosmos and came after Russian president Dmitry Medvedev threatened to punish those responsible for previous space failures, which included the loss of satellites and botched launches.”

In the meantime, let’s focus on the positive contributions the Russians have made towards lunar exploration – in particular, the Luna missions which set many milestones. Of these, they were the first to successfully land a craft of the Moon, the first to photograph the far side, the first to achieve a soft landing and send back panoramic, close-up images, the first to become an artificial lunar satellite, the first to deploy rover missions and the first to return lunar soil samples which they shared with the international scientific community.

Russia? Keep talking… Spasiba for your contributions!

Original Story Source: Fox DC News.

Posted on by Nancy Atkinson

The Eagle Nebula as You’ve Never Seen it Before

A new look at M16, the Eagle Nebula in this composite from the Herschel telescope in far-infrared and XMM-Newton in X-ray. Credits: far-infrared: ESA/Herschel/PACS/SPIRE/Hill, Motte, HOBYS Key Programme Consortium; X-ray: ESA/XMM-Newton/EPIC/XMM-Newton-SOC/Boulanger

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Here’s a stunning new look deep inside the iconic “Pillars of Creation.” As opposed to the famous Hubble Space Telescope image (below) — which shows mainly the surface of the pillars of gas and dust — this composite image from ESA’s Herschel Space Observatory in far-infrared and XMM-Newton telescope in X-rays allows astronomers to peer inside the pillars and see more detail of the structures in this region. It shows how the hot young stars detected by the X-ray observations are carving out cavities, sculpting and interacting with the surrounding ultra-cool gas and dust.

But enjoy the view while you can. The sad part is that likely, this beautiful region has already been destroyed by a supernova 6,000 years ago. But because of the distance, we haven’t seen it happen yet.

Gas Pillars in the Eagle Nebula
Gas Pillars in the Eagle Nebula, as seen by the Hubble Space Telescope. Credit: NASA/ESA/STScI, Hester & Scowen (Arizona State University)

The Eagle Nebula is 6,500 light-years away in the constellation of Serpens. It contains a young hot star cluster, NGC6611, which is visible with modest back-yard telescopes. This cluster is sculpting and illuminating the surrounding gas and dust, resulting in a huge hollowed-out cavity and pillars, each several light-years long.

The Hubble image hinted at new stars being born within the pillars, deep inside small clumps known as ‘evaporating gaseous globules’ or EGGs, but because of the obscuring dust, Hubble’s visible light picture was unable to see inside and prove that young stars were indeed forming.

The new image shows those hot young stars are responsible for carving the pillars.

The new image also uses data from near-infrared images from the European Southern Observatory’s (ESO’s) Very Large Telescope at Paranal, Chile, and visible-light data from its Max Planck Gesellschaft 2.2m diameter telescope at La Silla, Chile. All the individual images are below:

M16 seen in several different wavelengths. Credits: far-infrared: ESA/Herschel/PACS/SPIRE/Hill, Motte, HOBYS Key Programme Consortium; ESA/XMM-Newton/EPIC/XMM-Newton-SOC/Boulanger; optical: MPG/ESO; near-infrared/VLT/ISAAC/McCaughrean & Andersen/AIP/ESO

Earlier mid-infrared images from ESA’s Infrared Space Observatory and NASA’s Spitzer, and the new XMM-Newton data, have led astronomers to suspect that one of the massive, hot stars in NGC6611 may have exploded in a supernova 6,000 years ago, emitting a shockwave that destroyed the pillars. But we won’t see the destruction for several hundred years yet.

Source: ESA

Posted on by Jason Major

A Space Moonrise (and the PromISSe of a New Future)

The Moon rises above (below?) Earth's limb in this view from the ISS. (ESA/NASA)

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“The moon looks the same from the ISS as it does on Earth. Only we see it rise and set again and again.”

ESA astronaut André Kuipers tweeted this message earlier today, accompanied by the wonderful photo above showing a distant Moon resting along Earth’s limb. The solar panels of the docked Soyuz TMA-03M spacecraft are seen in the foreground.

André arrived at the Space Station on December 23 along with Expedition 30 crewmates Oleg Kononeko and Don Pettit.

In addition to conducting over 45 experiments for ESA, NASA and JAXA during his five months in orbit, André’s PromISSe mission will help educate children about math, science, engineering, technology, and the benefits – and challenges – of working in space.

The program will also encourage the next generation of space explorers to stay fit with the second edition of the international fitness initiative Mission X: Train Like an Astronaut.

A medical doctor, André serves as flight engineer aboard the ISS and will be highly involved in docking procedures for the new Dragon (SpaceX) and Cygnus (Orbital Sciences) capsules as part of NASA’s next-generation commercial spaceflight program.

Read ESA’s PromISSe mission blog here, and follow André Kuipers on Twitter @astro_andre for more Expedition 30 mission updates.

Posted on by Nancy Atkinson

New Crew Arrives Safely at International Space Station

Three international travelers arrived safely at the International Space Station in their Soyuz TMA-03M spacecraft, docking just in time for the holidays, at 15:19 UTC on December 23, 2011. Oleg Kononenko from Russia, NASA astronaut Don Pettit and European Space Agency astronaut Andre Kuipers from The Netherlands docked at the Rassvet module on the Russian segment of the complex, and a few hours later were greeted by three other crew members on the outpost, station Commander Dan Burbank of NASA and Russian Flight Engineers Anton Shkaplerov and Anatoly Ivanishin, who have been aboard the orbital laboratory for just over a month.
Continue reading “New Crew Arrives Safely at International Space Station”

Posted on by VirtualAstro

New Plans for ESA’s Experimental Re-entry Vehicle

ESA’s new IXV (Intermediate eXperimental Vehicle) Credit: ESA

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ESA and Arianespace have signed a contract planning the launch of ESA’s new IXV (Intermediate eXperimental Vehicle) on Europe’s new Vega Rocket in 2014. Vega is Europe’s new small launch system and it is designed to complement the heavy Ariane 5 and medium Soyuz Rocket systems launched from French Guiana.

The small rocket is capable of a wide range of payloads up to 1.5 tonnes, compared to Ariane 5 which can lift 20 tonnes, making it especially suitable for the commercial space market. The Vega Rocket will launch the IXV into a suborbital trajectory from Europe’s Spaceport in French Guiana, IXV will then return to Earth as if from a low-orbit mission, to test and qualify new critical technologies for future re-entry vehicles.

Vega Rocket Credit: Arianespace

The IXV will reach a velocity of 7.5km/s at an altitude of around 450km and then re-enter the Earth’s atmosphere gathering data about its flight. The vehicle will encounter hypersonic and supersonic speeds and will be controlled with complex avionics, thrusters and flaps.

Once the vehicle’s speed has been reduced enough, it will deploy a parachute, descend and land safely in the Pacific Ocean.

This flight will record data for the next five VERTA missions (Vega Research and Technology Accompaniment – Programme), which will demonstrate the systems re-usable versatility.

Two launches a year are planned for the new programme and construction of infrastructure including mission control and communications networks is currently underway.

Development and completion of the design, manufacturing and assembly is now underway for a flight window between January and September 2014.

VERTA (Vega Research and Technology Accompaniment – Programme) Credit: Arianespace

Source: ESA

Posted on by Tammy Plotner

Mars Express Reveals Possible Martian Glaciers

Phlegra Montes is a range of gently curving mountains and ridges on Mars. They extend from the northeastern portion of the Elysium volcanic province to the northern lowlands. The High-Resolution Stereo Camera on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465. This perspective view has been calculated from the Digital Terrain Model derived from the stereo channels. Credits: ESA/DLR/FU Berlin (G. Neukum)

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When it comes to exploring Mars, one of the greatest needs future astronauts will face is water. Why? Simple enough. Transporting water would take a huge amount of fuel. Now the Mars Express has imaged an area on the red planet which may yield large quantities of sub-surface ice. Its name is Phlegra Montes…

Extending from the northeastern portion of the Elysium volcanic province to the northern lowlands, spanning latitudes from roughly 30°N to 50°N, the Phlegra Montes are a gently rolling series of hills that have been probed by radar. It is surmised these low mountain ranges are not volcanic in origin, but created through tectonic forces and may conceal a copious supply of frozen water.

Thanks to high resolution stereo imaging from ESA’s Mars Express orbiter, we’re able to detect a feature called ‘lobate debris aprons’. They appear to surround almost every mountain in the Phelegra’s and it’s a normal feature for mountains found around these latitudes. Earlier studies of the debris aprons show the material has slid down the mountain slopes with time – a feature shared with Earth’s glaciers. Because of this similarity, scientists surmise this region may be a type of Martian glacier. It’s a guess that’s also been confirmed by radar on NASA’s Mars Reconnaissance Orbiter.

Phlegra Montes is a range of gently curving mountains and ridges on Mars. Flow patterns attributable to water are widely visible across the image. Linear flow patterns can be seen inside the valley (Box 1). Nearly every mountain is surrounded by an apron of rocky debris (Box 2). Over time, this debris appears to have moved down the mountainside and looks similar to the debris found covering glaciers here on Earth. Lobe-shaped structures seen inside impact craters in the region (Box 3) are known as concentric crater fill and are perhaps another indication of subsurface water ice. The High-Resolution Stereo Camera on ESA’s Mars Express collected the data for these images on 1 June 2011 during orbit 9465. Credits: ESA/DLR/FU Berlin (G. Neukum)

According to the radar data, the lobate debris aprons could indeed signal the presence of ice – perhaps only 20 meters below the surface. To further confirm their findings, nearby impact craters also show signs of recent glaciation. It would appear that ridges formed inside these ancient holes from snowfall, and then slid down the slopes. With time, it compacted to form a glacier structure… and even more glacier flow patterns are visible in the valleys.

How did this come to be? A one time, Mars’ polar axis was quite different than it is today. As it changed, it created different climatic conditions and mid-latitude glaciers may have developed at different times over the last several hundred million years. While you might be tired of hearing about water on Mars, the findings are very exciting for the future of exploration. It means the door is open…

And one day we just might go through it!

Original Story Source: ESA News.

Posted on by Tammy Plotner

“Star Wars” Laser Methods Tracks Greenhouse Gases

A green laser was used to guide the invisible infrared beam from La Palma to Tenerife as part of an experiment to test a new satellite concept for measuring atmospheric greenhouse gases and turbulence. Credits: ESA

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It may have looked like a futuristic scene from Star Wars, but ESA’s latest technique for aiding space exploration might shed some “green light” on greenhouse gases. A recent experiment involving the Spanish Canary Islands was conducted by shooting laser beams from a peak on La Palma to Tenerife. The two-week endeavor not only increased the viability of using laser pulses to track satellites, but increased our understanding of Earth’s atmosphere.

ESA runs an optical ground station in Tenerife for communications links with satellites. The facility is part of a larger astronomical installation Observatorio del Teide run by Instituto de Astrofisica de Canarias. Credit: ESA
Known as infrared differential absorption spectroscopy, the laser method is an accurate avenue to measure trace gases such as carbon dioxide and methane. It is accomplished by linking two Earth-orbiting satellites – one a transmitter and the other a receiver – and examining the atmosphere as the beam passes between the two. As satellites orbit, they both rise and set behind Earth and radio occultation occurs. It’s a time-honored way of employing microwave signals to measure Earth’s atmosphere, but new wave thinking employs shortwave infrared laser pulses. When the correct wavelength is achieved, the atmospheric molecules impact the beam and the resultant data can then be used to establish amounts of trace gases and possibly wind. By different angular repetitions, a vertical picture can be painted which stretches between the lower stratosphere to the upper troposphere.

While it all sounded good on paper – the proof of a working model is when it is tested. Enter ESA’s optical ground station on Tenerife – a facility built on a peak 2390 meters above sea level and part of a larger astronomical installation called the Observatorio del Teide run by the Instituto de Astrofisica de Canarias (IAC).With equipment placed on two islands, the Tenerife location offered the perfect setting to install receiver hardware grafted to the main telescope. The transmitter was then assigned to a nearly identical peak on La Palma. With nothing but 144 kilometers of ocean between them, the scenario was ideal for experimentation.

Over the course of fourteen days, the team of researchers from the Wegener Center of the University of Graz in Austria and the Universities of York and Manchester in the UK were poised to collect this unique data.

The Observatorio del Roque de los Muchachos on the island of La Palma housed the equipment to transmit the infrared signal and green guidance laser across the Atlantic Ocean to the receiving station in Tenerife. The experiment was carried out to test a new satellite mission concept for measuring concentrations of atmospheric carbon dioxide and methane. Credit: ESA
While the infrared beam wasn’t visible to the unaided eye, the green guidance laser lit up the night during its runs to record atmospheric turbulence. Gottfried Kirchengast from the Wegener Center said, “The campaign has been a crucial next step towards realising infrared-laser occultation observations from space. We are excited that this pioneering inter-island demonstration for measuring carbon dioxide and methane was successful.”

Armin Loscher from ESA’s Future Mission Division added, “It was a challenging experiment to coordinate, but a real pleasure to work with the motivated teams of renowned scientists and young academics.” The experiment was completed within ESA’s Earth Observation Support to Science Element.

Nice shootin’!

Original Story Source: ESA News Release.

Posted on by Tammy Plotner

Cosmic Particle Accelerators – Let’s Dance!

Depicted in the composition are: a bow shock around the very young star, LL Ori, in the Great Orion Nebula (upper row, left image); shock waves around the Red Spider Nebula, a warm planetary nebula (upper row, central image); very thin shocks on the edge of the expanding supernova remnant SN 1006 (central row, left image); artist's impressions of the bow shock created by the Solar System as it moves through the interstellar medium of the Milky Way (upper row, right image) and of Earth's bow shock, formed by the solar wind as it encounters our planet's magnetic field (central row, right image); shock-heated shells of hot gas on the edge of the lobes of the radio galaxy Cygnus A (lower row, left image); a bow shock in the hot gas in the merging galaxy cluster 1E 0657-56, also known as the 'Bullet Cluster'.

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Are you ready to dance with a new discovery? ESA’s Cluster satellites are playing the tune of cosmic particle acceleration – and it’s more efficient than speculated. Now we’re taking a look at the beginnings of universal motion. By embracing a wide variety of astronomical targetry, the images are revealing shock waves where supersonic flows of plasma encounter everything from a slow flow to an irresistible force.

What sets things in motion? When it comes to particle accelerators, something needs to set it off. Here on Earth, the Large Hadron Collider (LHC) located at Cern uses a bank of smaller machines for giving rise to the charged particles before introducing them into the mainstream. In space, cosmic rays act as this “mainstream”, but they aren’t very efficient at setting the particles going initially. Now the ESA Cluster mission has revealed what could be ” natural particle accelerators of space”.

While cruising through a magnetic shock wave, the four Cluster satellites found themselves perfectly lined up with the magnetic field. This perfect chance alignment was a revelation – allowing the mission to sample the event with incredible accuracy on a very short timescale – one of 250 milliseconds or less. What surfaced from the investigation was the realization that the electrons heated rapidly, a state which contributes to acceleration on a greater scale. While this type of action had been speculated before, it hadn’t been observed or proved. No one really knew about the process or the size of the shock layers. With this new data, Steven J. Schwartz of the Imperial College London, and his colleagues were able to estimate the thickness of the shock layer – a significant advancement in understanding, because a thinner layer means faster acceleration.

“With these observations, we found that the shock layer is about as thin as it can possibly be,” says Professor Schwartz.

So just how skinny is this dance partner? Scientists had originally estimated the shock layers above Earth to be no more than 100 km, but the satellite information showed them to be about 17 km… a very fine detail!

Artist's impression of the four Cluster spacecraft flying through the thin layer of Earth's bow shock. The crossing, which took place on 9 January 2005, showed that the shock's width was only about 17 kilometres across.

This type of knowledge is significant simply because shocks exists universally – originating virtually everywhere a flow encounters an obstacle or another flow. For example, here in the Solar System the Sun generates a speedy, electrically charged stellar wind. When it runs headlong into a magnetic field – such as generated by Earth – it creates a shock wave located in front of the planet. Through the Cluster mission studies, we can apply what we learn here at home and extrapolate it on a grander scale – such as those created by supernovae events, black holes and galaxies. It might even reveal the origin of cosmic rays!

“This new result reveals the size of the proverbial ‘black box’, constraining the possible mechanisms within it involved in accelerating particles,” says Matt Taylor, ESA Cluster project scientist. “Yet again, Cluster has provided us with a clear insight into a physical process that occurs throughout the Universe.”

Come on, baby. Let’s dance…

Original Story Source: ESA News Release.

Posted on by Tammy Plotner

LISA Pathfinder – Surfing Gravity Waves

LISA Pathfinder about to enter the space environment vacuum test. Credit: ESA

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Do you remember the LISA mission? I do! The proposed launch for this unique vision is slated for 2014 and the latest sensor technology is making its own waves… by being far more accurate than expected. Now ESA’s LISA Pathfinder mission is better than ever, and ready to tackle the vast ocean of space in search of elusive gravitational waves…

So what’s new? By employing a near complete version of LISA, the Optical Meteorology Subsystem passed its first test under space-like temperature and vacuum conditions. Not only did it make the grade, but it went far beyond. It surpassed the precision requirement needed to detect gravitational waves by 300%!

Einstein predicted them, but to physically record this phenomenon in space, the LISA Pathfinder will utilize a laser to measure the distance between two free-floating gold–platinum cubes. Here on the ground, the team in Ottobrunn, Germany, are performing the tests using mirrors instead of cubes. Not only will the distance between them be cataloged, but their angles with respect to the laser beams. Is LISA good? Darn right. She had an accuracy rating of 10 billionths of a degree!

LISA Pathfinder with scientists in the clean room test environment. Credits: Astrium UK
“This is equivalent to the angle subtended by an astronaut’s footprint on the Moon!” notes Paul McNamara, Project Scientist for the LISA Pathfinder mission.

So how are gravitational waves detected? If perfect conditions do exist in space, then the free-floating cubes should mirror each other’s motions. Now, enter Einstein’s general theory of relativity. If some gravitational event should occur – such as the collision of two black holes – this should cause a minute distortion in the fabric of space. These tiny changes should be detectable. However, the accuracy needed to record such an event would need to be about one hundredth the size of an atom… a size called a “picometre”. Originally, LISA was optimized at 6 picometres measured over a timeline of 1000 seconds. But she bettered her record in 2010 and has now reached an amazing accuracy level of 2 picometres.

“The whole team has worked extremely hard to make this measurement possible,” said Dr McNamara. “When LISA Pathfinder is launched and we’re in the quiet environment of space some 1.5 million km from Earth, we expect that performance will be even better.”

Final preparation work on LISA Pathfinder ahead of the space environment testing. Credits: Astrium UK
The instrument team from Astrium GmbH, the Albert Einstein Institute and ESA are testing the Optical Metrology Subsystem during LISA Pathfinder thermal vacuum tests in Ottobrunn by spacecraft prime contractor Astrium (UK) Ltd. Tentatively set to launch in mid-2014, the LISA Pathfinder is well on its way to ride the gravitational waves and set the pace for ESA’s New Gravitational Wave Observatory. Perhaps within the next 10 years we’ll see even more advancements in finding the “final piece in Einstein’s cosmic puzzle.”

Way to go, LISA!

Original Story Source: ESA News Release.

Posted on by Ray Sanders

New ESA Images Reveal Volcanic History of Mars

Tharsis Tholus towers 8 km above the surrounding terrain. Its base stretches 155 x 125 km. What makes Tharsis Tholus unusual is its extremely battered condition. Image Credit: ESA/DLR/FU Berlin (G. Neukum)

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Earlier this week, The European Space Agency released new Mars images taken by instruments aboard the Mars Express spacecraft. The images show details of Tharsis Tholus, which appears to be a very large and extinct volcano that has been battered and deformed over time.

On Earth, Tharsis Tholus would be a towering giant of a volcano, looming 8 km above the surrounding terrain, with a base of roughly 155 x 125 km. Despite its size, Tharsis Tholus is just an average run-of-the-mill volcano on Mars. That being said, it isn’t the size of Tharsis Tholus that makes it interesting to scientists – what makes the remnants of this volcano stand out is its extremely battered condition.

What does the battered condition of Tharsis Tholus mean to planetary scientists studying Mars?

Details shown in the image above by the HRSC high-resolution stereo camera on ESA’s Mars Express spacecraft reveal signs of dramatic events which have significantly altered the volcanic region of Tharsis Tholus. Two (or more) large sections have collapsed around its eastern and western regions in the past several billion years, leaving signs of erosion and faulting.

One main feature of Tharsis Tholus that stands out is the volcanic caldera in its center. The caldera is nearly circular, roughly 30 km across and ringed by faults that have allowed the floor of the caldera to subside by nearly 3km. Planetary scientists believe the volcano emptied its magma chamber during eruptions. Once the magma chamber had emptied its lava onto the surface, the chamber roof became unstable under its own weight and collapsed, forming the large caldera.

This image was created using a Digital Terrain Model (DTM) obtained from the High Resolution Stereo Camera on ESA’s Mars Express spacecraft. Elevation data from the DTM is colour coded: purple indicates the lowest lying regions and beige the highest. Image Credit: ESA/DLR/FU Berlin (G. Neukum)

This month is a very busy month for Mars exploration. Russia’s recently launched (and in distress) Phobos mission (Mission coverage at: http://www.universetoday.com/90808/russians-race-against-time-to-save-ambitious-phobos-grunt-mars-probe-from-earthly-demise/) has a mission goal of returning a sample from Mars’ moon, Phobos, along with “piggyback” missions by China and the Planetary Society.

NASA’s plans to launch the Mars Science Laboratory on November 25th (Coverage at: http://www.universetoday.com/90639/curiosity-rover-bolted-to-atlas-rocket-in-search-of-martian-microbial-habitats/). MSL consists of the “Curiosity” rover and will be performing experiments designed to detect organic molecules, which may help detect signs of past or present life on Mars.

This month also marks the end of the “Mars500” mission, which ended on Friday (coverage at: http://www.universetoday.com/90554/mars500-crew-ready-to-open-hatch/ when the participants opened their hatch for the first time since June 2010. During the past 520 days, the participants were working in a simulated spacecraft environment in Moscow.

Learn more about Mars Express at: http://www.esa.int/esaMI/Mars_Express/index.html

Source: ESA Press Release